“…The obtention of input energy spectra offers an important advantage to determine the energy input to structures with the effect of ground motions. Peak ground acceleration, peak ground velocity, the ratio of peak ground acceleration to peak ground velocity, the duration and predominant periods of ground motions, fault type and mechanism, distance to the fault, the magnitude of ground motions and soil conditions were referred in many previous studies as specific parameters to obtain the seismic input energy spectra [19,25,28,[37][38][39][40][41][42][43][44]. Fajfar and Vidic [37], Sucuoglu and Nurtug [38], Decanini and Mollaioli [39], Manfredi [24], Benavent-Climent et al [40], López-Almansa et al [41], Dindar et al [42], Quinde et al [43], Alici and Sucuoglu [44] and Ozsarac et al [45] made pioneer and further investigations about the earthquake input energy spectra for both elastic and inelastic systems.…”